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The continents appear to have once fit together (like South America and Africa). Also, there were similar fossils found on different continents.
Lenticular clouds form near mountains
Pangaea, also known as the Supercontinent, is the land mass that may have existed at about 250 million years ago. It was a single land mass that consisted of all of the continents, which have since drifted to their current positions. The idea of Pangaea was first proposed by Alfred Wegener. Evidence pointing to the existence of Pangaea includes similarities in fossils and rocks on continents which are now far away and that the coastlines of some of today's continents appear to fit together like puzzle pieces.
It is a weathered granite landscape consisting of tors, which appear as jumbled, sometimes precariously balanced rocks, usually near a hilltop.
540 Million years ago
The continents appear to have once fit together (like South America and Africa). Also, there were similar fossils found on different continents.
Glaciers have appeared on every continent except Australia. They have been particularly extensive in Antarctica, Greenland, North America, and Europe during past glaciations.
Wegner developed this theory not only because many continents appear to fit together like a jigsaw, but also because he had fossil and climate evidence to support the fact that the continents once fit together.
I don't think they do.
In the North America
yes!
yes!
Lenticular clouds form near mountains
Because many of the rock formations appear to have been man made from a distance.
There is no evidence that Silver Surfer will appear.
The continents of the Earth are not included in the part of the original crust because they appear differently. These continents used to all be one large continent called Pangaea.
One piece of evidence that the continents were once together is the matching shapes of their coastlines, particularly noticeable with South America and Africa fitting together like puzzle pieces. This phenomenon supports the theory of continental drift proposed by Alfred Wegener during the early 20th century.